Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi
The works is made on the base of the materials collected during two field phases (2013-2014) in the territory of the R-41-XX, XXI sheet (Amderma area). Visean-Serpuhovian bathyal sediments of Pai-Khoi Shale Belt are represented by Kara formation. In contrast to the underlying and overlying predomina...
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Sergo Ordzhonikidze Russian State University for Geological Prospecting
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ftdoajarticles:oai:doaj.org/article:bf14413c773b41dd9375b04fdf05d4c0 2023-05-15T13:21:38+02:00 Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi K. P. Ryazanov 2015-12-01T00:00:00Z https://doi.org/10.32454/0016-7762-2015-6-21-27 https://doaj.org/article/bf14413c773b41dd9375b04fdf05d4c0 RU rus Sergo Ordzhonikidze Russian State University for Geological Prospecting https://www.geology-mgri.ru/jour/article/view/85 https://doaj.org/toc/0016-7762 https://doaj.org/toc/2618-8708 0016-7762 2618-8708 doi:10.32454/0016-7762-2015-6-21-27 https://doaj.org/article/bf14413c773b41dd9375b04fdf05d4c0 Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 21-27 (2015) тип слоя циклотема белые курильщики сипы трансгрессивно-регрессивный цикл Geology QE1-996.5 article 2015 ftdoajarticles https://doi.org/10.32454/0016-7762-2015-6-21-27 2023-03-19T01:40:27Z The works is made on the base of the materials collected during two field phases (2013-2014) in the territory of the R-41-XX, XXI sheet (Amderma area). Visean-Serpuhovian bathyal sediments of Pai-Khoi Shale Belt are represented by Kara formation. In contrast to the underlying and overlying predominantly clayey-siliceous sediments, it is composed of carbonate rocks. This study is focused on composition and origin of the carbonate sediments of the Kara formation in North East Pai-Khoi and is based on the analysis of cyclic sedimentary rock associations - cyclothems. The upper part of the formation section encloses two cyclothem types: fourth type is a sedimentation sequence, which is adequate to the development cycle of hydrothermal structures («white smokers»); the fifth type is represented by so-caffed seeps or nucleuses of fluid flows leakage on continental margins. The deeper section is formed by the activity of the carbonated turbidites. Finally, the formational model of Kara formation (Mississippian period) of North East Pai-Khoi is constmcted, which is considered to be responsible of the sedimentation sequence. Article in Journal/Newspaper Amderma Directory of Open Access Journals: DOAJ Articles Amderma ENVELOPE(61.666,61.666,69.758,69.758) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
тип слоя циклотема белые курильщики сипы трансгрессивно-регрессивный цикл Geology QE1-996.5 |
spellingShingle |
тип слоя циклотема белые курильщики сипы трансгрессивно-регрессивный цикл Geology QE1-996.5 K. P. Ryazanov Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
topic_facet |
тип слоя циклотема белые курильщики сипы трансгрессивно-регрессивный цикл Geology QE1-996.5 |
description |
The works is made on the base of the materials collected during two field phases (2013-2014) in the territory of the R-41-XX, XXI sheet (Amderma area). Visean-Serpuhovian bathyal sediments of Pai-Khoi Shale Belt are represented by Kara formation. In contrast to the underlying and overlying predominantly clayey-siliceous sediments, it is composed of carbonate rocks. This study is focused on composition and origin of the carbonate sediments of the Kara formation in North East Pai-Khoi and is based on the analysis of cyclic sedimentary rock associations - cyclothems. The upper part of the formation section encloses two cyclothem types: fourth type is a sedimentation sequence, which is adequate to the development cycle of hydrothermal structures («white smokers»); the fifth type is represented by so-caffed seeps or nucleuses of fluid flows leakage on continental margins. The deeper section is formed by the activity of the carbonated turbidites. Finally, the formational model of Kara formation (Mississippian period) of North East Pai-Khoi is constmcted, which is considered to be responsible of the sedimentation sequence. |
format |
Article in Journal/Newspaper |
author |
K. P. Ryazanov |
author_facet |
K. P. Ryazanov |
author_sort |
K. P. Ryazanov |
title |
Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
title_short |
Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
title_full |
Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
title_fullStr |
Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
title_full_unstemmed |
Genetic model of the Kara formation (Lower Carbonniferous) ofNorth-Easternpartofthe ridge of Pai-Khoi |
title_sort |
genetic model of the kara formation (lower carbonniferous) ofnorth-easternpartofthe ridge of pai-khoi |
publisher |
Sergo Ordzhonikidze Russian State University for Geological Prospecting |
publishDate |
2015 |
url |
https://doi.org/10.32454/0016-7762-2015-6-21-27 https://doaj.org/article/bf14413c773b41dd9375b04fdf05d4c0 |
long_lat |
ENVELOPE(61.666,61.666,69.758,69.758) |
geographic |
Amderma |
geographic_facet |
Amderma |
genre |
Amderma |
genre_facet |
Amderma |
op_source |
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 21-27 (2015) |
op_relation |
https://www.geology-mgri.ru/jour/article/view/85 https://doaj.org/toc/0016-7762 https://doaj.org/toc/2618-8708 0016-7762 2618-8708 doi:10.32454/0016-7762-2015-6-21-27 https://doaj.org/article/bf14413c773b41dd9375b04fdf05d4c0 |
op_doi |
https://doi.org/10.32454/0016-7762-2015-6-21-27 |
_version_ |
1766360713829285888 |